The passenger ship, which travels between the lake centers in the course of the season, is also suitable for exploring Lake Altmühlsee in a relaxed manner. A shipping line on which the MS Altmühlsee operates connects the three lake centers (Wald, Muhr am See and Schlungenhof). Weißenburg-Gunzenhausen district: Northern and western part of the district, with the communities of Absberg, Alesheim, Muhr a.See, Bergen, Burgsalach, Dittenheim, Ellingen, Ettenstatt, Gnotzheim, Gunzenhausen, Haundorf, Heidenheim, Höttingen, Markt Berolzheim, Meinheim, Nennslingen, Pfofeld, Pleinfeld, Polsingen, Raitenbuch, Theilenhofen and Westheim. In: Historic Atlas of Bavaria, part of Franconia. From here the Altmühl is a part of the primary-Danube Canal, which is accompanied on this route on the left and right by quite a few remnants of its predecessor, the Ludwig-Donau-Principal Canal, some of which are also linked to it. From here, the Altmühl flows in an synthetic course on a larger scale roughly east-southeast to the japanese circulate across the Altmühlsee. Section additionally runs underground under the left edge of the Altmühltal, to the Kleiner Brombachsee in the Rednitz catchment area. Schafgraben, from the left and northwest to under 418 m above sea level.

Hesselbach, from the left and north-northeast to under 418 m above sea level. The decrease Schlegelsbühlgraben takes the higher Bankertsgraben from the left and northwest to beneath 414.9 m above sea level. Judengraben, from the left and northwest at round 414 m above sea degree. This floodplain ditch is the right branch of the previous one at round 414 m above sea degree. Drains in a similar meandering course as the Fallach mentioned above to below 414 m above sea stage. Arises under 420 m above sea level. Arises at round 420 m above sea stage. Flows at about 420 m above sea stage. Wieseth, from the best and southeast or southwest to beneath 416 m above sea level. Roßbachgraben, from the proper and west at 416.7 m above sea level. → Exit of the Kaltenlachgraben, to the fitting and south to 414.7 m above sea level. → Departure of the Schlegelsbühlgraben secondary stream, also called Häfelesgraben, at below 414.9 m above sea level. Northeast at under 418 m above sea stage. Arises at around 418 m above sea level. Arises at over 418 m above sea stage. Ant ditch, from the left and north-northwest at 418 m above sea level. Betzengraben, from the left and north to over 416 m above sea stage. Fallach coming from the north (see above) and the Zegelgraben coming from the west on the right; The last one arises straight on the Altmühl feeder and seems to be the lower reaches of an outdated proper estuary of the Wieseth, which is now not steady on account of the development of the Altmühl feeder, as a result of the Zeckl, Zegel or Leugraben flows to the other aspect of the feeder, which now flows is initiated into this.

Within the Franconian Lake District the path continues to Wolframs-Eschenbach, Merkendorf and above Ornbau over the Altmühl and Wieseth rivers to Arberg. The Wieseth flows into two branches, the main department north of the mill, the secondary department about 500 meters west of it. The two higher reaches as much as the Heidweiher are also known as Wiesengraben. There are additionally two moats in course of the end of the mountain spur, considered one of which remains to be six meters deep. NN at a dirt highway junction west of Dittenheim-Sammenheim. NN inside the local space, barely offset in front of a dry valley mouth from the course of Riedenburg--Perletzhofen, from the place supply from sinkholes has been confirmed. Generally karstification additionally results in the formation of a lake district, such as the Plitvice Lake District. Bimswinkelgraben, from the left and west to beneath 416 m above sea degree. Raingraben, from the left and north at over 416 m above sea stage. North at over 405 m above sea degree. Heglauer Mühlbach, from the left and north at over 414.7 m above sea level. Inlet of the Heidental dry valley, from the left and north at 338.2 m above sea stage.

Return of the Roßgraben, from the left and west-northwest to 414.9 m above sea stage. NN on the northwest seaside of Unterwurmbach only a hundred meters from the run of the previous one. State and folklore of the Kingdom of Bavaria. On account of the Reich Deputation Center and because of the secularization of the German order by Napoléon Bonaparte, the Öfelinsmühle as properly because the Birkenmühle and the Langweidmühle in 1806 handed to the new Kingdom of Bavaria. The list of landscapes in Bavaria is predicated on the numbering of the Federal Institute for Regional Studies. Kästleinsmühlbach, partly also called Schambach, from left and east to lower than 410 m above sea stage. → Departure of the Roßgraben, to the left and east southeast on the southern edge of orn building to 415.Three m above sea level. Part identify sequence Braungartenbach → Dümpfelgraben → Oberer Mühlbach → Heglauer Mühlbach. Part of the name Steingraben → Haidgraben (!) → Heidweiher → Heidweihergraben. Oberlauf sequence Dorfbach (by means of Esbach) → Birkengraben → Higher Kuhgraben → Decrease Kuhgraben → Betzengraben. Higher course from the origin of the Langwiesengraben and approx. Upper course and approx. 3.2 km². Arises beneath 365 m above sea level.


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